XFVM 模拟由剪切和拉伸开口引起的断裂孔径。

IF 2.1 3区 地球科学 Q3 COMPUTER SCIENCE, INTERDISCIPLINARY APPLICATIONS
Computational Geosciences Pub Date : 2024-01-01 Epub Date: 2023-07-25 DOI:10.1007/s10596-023-10214-5
Giulia Conti, Stephan Matthäi, Patrick Jenny
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引用次数: 0

摘要

在储层模拟中,了解裂缝岩石的力学行为以及裂缝的剪切和拉伸位移对其孔径的影响非常重要。拉伸张开会直接增大裂缝孔径,而对已存在的粗壁裂缝的剪切则会产生孔径变化,这种变化取决于当地的应力状态。由于裂缝扩张会增加储层渗透率,因此这两个过程都必须以现实和一致的方式纳入储层力学模拟模型。在此,我们使用扩展有限体积法(XFVM)进行流动和地质力学模拟。在 XFVM 中,裂缝被嵌入孔弹性矩阵中,并使用非连续基函数进行建模。在每个断裂段上计算牵引力和压缩力,并为剪切位移和拉伸位移增加一个额外的自由度。在这一特定的 XFVM 实现中,我们假定线性弹性和稳态流体压力充分约束了有效应力。在本文中,剪切扩张并不是事后计算的,而是进入方程,使孔径变化直接影响应力状态。这是通过在位移梯度中加入剪切扩张来实现的,因此可以确保应力-应变关系和力平衡的一致性。我们将在两个简单的测试案例中,以及在一个真实的受层限制的二维断裂网络中,在合理的原位应力和孔隙压力条件下,对这一额外项的影响进行说明和讨论。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

XFVM modelling of fracture aperture induced by shear and tensile opening.

XFVM modelling of fracture aperture induced by shear and tensile opening.

In reservoir simulation, it is important to understand the mechanical behaviour of fractured rocks and the effect of shear and tensile displacements of fractures on their aperture. Tensile opening directly enhances the fracture aperture, whereas shear of a preexisting rough-walled fracture creates aperture changes dependent on the local stress state. Since fracture dilatation increases reservoir permeability, both processes must be included in a realistic and consistent manner into the mechanical reservoir simulation model. Here, we use the extended finite volume method (XFVM) to conduct flow and geomechanics simulations. In XFVM, fractures are embedded in a poroelastic matrix and are modelled with discontinuous basis functions. On each fracture segment the tractions and compressive forces are calculated, and one extra degree of freedom is added for both the shear and tensile displacement. In this particular XFVM implementation we assume that linear elasticity and steady state fluid pressure adequately constrain the effective stress. In this paper, shear dilation is not calculated a posteriori, but it enters the equations such that aperture changes directly affect the stress state. This is accomplished by adding shear dilation to the displacement gradients and therefore ascertains a consistent representation in the stress-strain relations and force balances. We illustrate and discuss the influence of this extra term in two simple test cases and in a realistic layer-restricted two-dimensional fracture network subjected to plausible in situ stress and pore pressure conditions.

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来源期刊
Computational Geosciences
Computational Geosciences 地学-地球科学综合
CiteScore
6.10
自引率
4.00%
发文量
63
审稿时长
6-12 weeks
期刊介绍: Computational Geosciences publishes high quality papers on mathematical modeling, simulation, numerical analysis, and other computational aspects of the geosciences. In particular the journal is focused on advanced numerical methods for the simulation of subsurface flow and transport, and associated aspects such as discretization, gridding, upscaling, optimization, data assimilation, uncertainty assessment, and high performance parallel and grid computing. Papers treating similar topics but with applications to other fields in the geosciences, such as geomechanics, geophysics, oceanography, or meteorology, will also be considered. The journal provides a platform for interaction and multidisciplinary collaboration among diverse scientific groups, from both academia and industry, which share an interest in developing mathematical models and efficient algorithms for solving them, such as mathematicians, engineers, chemists, physicists, and geoscientists.
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